Editorial Type:
Article
Article Type:
Research Article

Streamflow Data from Small Basins: A Challenging Test to High-Resolution Regional Climate Modeling

Kerstin Stahl Department of Geosciences, University of Oslo, Oslo, Norway, and Institute of Hydrology, University of Freiburg, Freiburg, Germany

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Lena M. Tallaksen Department of Geosciences, University of Oslo, Oslo, Norway

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Lukas Gudmundsson Department of Geosciences, University of Oslo, Oslo, Norway

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Jens H. Christensen Danish Meteorological Institute, Copenhagen, Denmark

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Print Publication:
01 Oct 2011
Collections:
Water and Global Change (WATCH) Special Collection
DOI:
https://doi.org/10.1175/2011JHM1356.1
Page(s):
900–912
Restricted access

Abstract

Land surface models and large-scale hydrological models provide the basis for studying impacts of climate and anthropogenic changes on continental- to regional-scale hydrology. Hence, there is a need for comparison and validation of simulated characteristics of spatial and temporal dynamics with independent observations. This study introduces a novel validation framework that relates to common hydrological design measures. The framework is tested by comparing anomalies of runoff from a high-resolution climate-model simulation for Europe with a large number of streamflow observations from small near-natural basins. The regional climate simulation was performed as a “poor man’s reanalysis,” involving a dynamical downscaling of the 40-yr European Centre for Medium-Range Weather Forecasts Re-Analysis (ERA-40) with the Danish “HIRHAM5” model. For 19 different anomaly levels, two indices evaluate the temporal agreement (i.e., the occurrence and frequency of dry and wet events based on daily anomalies), whereas two other indices compare the interannual variability and trends based on annual anomalies. Benchmarks on each index facilitated a comparison across indices, anomaly levels, and basins. The lowest agreement of observed and simulated anomalies was found for dry anomalies. Weak to moderately wet anomalies agreed best, but agreement dropped again for the wettest anomalies. The results could guide the decision on thresholds if this regional climate model were used for the assessment of climate change scenario impacts on flood and drought statistics. Indices vary across Europe, but a gradient with decreasing correspondence between observed and simulated runoff characteristics from west to east, from lower to higher elevations, and from fast to slowly responding basins can be distinguished. The suggested indices can easily be adapted to other study areas and model types to assist in assessing the reliability of predictions of hydrological change.

Corresponding author address: Kerstin Stahl, Dept. of Geosciences, University of Oslo, P.O. Box 1047, Blindern, NO-0316 Oslo, Norway. E-mail: kerstin.stahl@geo.uio.no

This article is included in the Water and Global Change (WATCH) special collection.

Abstract

Land surface models and large-scale hydrological models provide the basis for studying impacts of climate and anthropogenic changes on continental- to regional-scale hydrology. Hence, there is a need for comparison and validation of simulated characteristics of spatial and temporal dynamics with independent observations. This study introduces a novel validation framework that relates to common hydrological design measures. The framework is tested by comparing anomalies of runoff from a high-resolution climate-model simulation for Europe with a large number of streamflow observations from small near-natural basins. The regional climate simulation was performed as a “poor man’s reanalysis,” involving a dynamical downscaling of the 40-yr European Centre for Medium-Range Weather Forecasts Re-Analysis (ERA-40) with the Danish “HIRHAM5” model. For 19 different anomaly levels, two indices evaluate the temporal agreement (i.e., the occurrence and frequency of dry and wet events based on daily anomalies), whereas two other indices compare the interannual variability and trends based on annual anomalies. Benchmarks on each index facilitated a comparison across indices, anomaly levels, and basins. The lowest agreement of observed and simulated anomalies was found for dry anomalies. Weak to moderately wet anomalies agreed best, but agreement dropped again for the wettest anomalies. The results could guide the decision on thresholds if this regional climate model were used for the assessment of climate change scenario impacts on flood and drought statistics. Indices vary across Europe, but a gradient with decreasing correspondence between observed and simulated runoff characteristics from west to east, from lower to higher elevations, and from fast to slowly responding basins can be distinguished. The suggested indices can easily be adapted to other study areas and model types to assist in assessing the reliability of predictions of hydrological change.

Corresponding author address: Kerstin Stahl, Dept. of Geosciences, University of Oslo, P.O. Box 1047, Blindern, NO-0316 Oslo, Norway. E-mail: kerstin.stahl@geo.uio.no

This article is included in the Water and Global Change (WATCH) special collection.

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